<rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dct="http://purl.org/dc/terms/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#">
  <rdf:Description rdf:about="https://doi.org/PMC8824702">
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    <dct:isPartOf>National Science Review</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2021-06-29</dct:created>
    <dc:description>Abstract                &lt;p&gt;Widespread soil acidification due to atmospheric acid deposition and agricultural fertilization may greatly accelerate soil carbonate dissolution and CO2 release. However, to date, few studies have addressed these processes. Here, we use meta-analysis and nationwide-survey datasets to investigate changes in soil inorganic carbon (SIC) stocks in China. We observe an overall decrease in SIC stocks in topsoil (0&#65506;&#65408;&#65427;30&#65474;&#65440;cm) (11.33&#65474;&#65440;g C m&#65506;&#65408;&#65427;2 yr&#65506;&#65408;&#65427;1) from the 1980s to the 2010s. Total SIC stocks have decreased by &#65506;&#65416;&#65468;8.99&#65474;&#65440;&#65474;&#65457;&#65474;&#65440;2.24% (1.37&#65474;&#65440;&#65474;&#65457;&#65474;&#65440;0.37&#65474;&#65440;Pg C). The average SIC losses across China (0.046 Pg C yr&#65506;&#65408;&#65427;1) and in cropland (0.016 Pg C yr&#65506;&#65408;&#65427;1) account for &#65506;&#65416;&#65468;17.6%&#65506;&#65408;&#65427;24.0% of the terrestrial C sink and 57.1% of the soil organic carbon sink in cropland, respectively. Nitrogen deposition and climate change have profound influences on SIC cycling. We estimate that &#65506;&#65416;&#65468;19.12%&#65506;&#65408;&#65427;19.47% of SIC stocks will be further lost by 2100. The consumption of SIC may offset a large portion of global efforts aimed at ecosystem carbon sequestration, which emphasizes the importance of achieving a better understanding of the indirect coupling mechanisms of nitrogen and carbon cycling and of effective countermeasures to minimize SIC loss.&lt;/p</dc:description>
    <dc:subject>Carbon sequestration</dc:subject>
    <dc:subject>Cartography</dc:subject>
    <dc:subject>China</dc:subject>
    <dc:subject>Mechanics and Transport in Unsaturated Soils</dc:subject>
    <dc:subject>Carbonate</dc:subject>
    <dc:subject>Nitrogen</dc:subject>
    <dc:subject>Soil Science</dc:subject>
    <dc:subject>Organic chemistry</dc:subject>
    <dc:subject>Carbon Dynamics in Peatland Ecosystems</dc:subject>
    <dc:subject>soil inorganic carbon stocks</dc:subject>
    <dc:subject>Soil pH</dc:subject>
    <dc:subject>Environmental science</dc:subject>
    <dc:subject>Carbon sink</dc:subject>
    <dc:subject>Agricultural and Biological Sciences</dc:subject>
    <dc:subject>carbonate</dc:subject>
    <dc:subject>Engineering</dc:subject>
    <dc:subject>Soil water</dc:subject>
    <dc:subject>Soil Carbon Sequestration</dc:subject>
    <dc:subject>Biology</dc:subject>
    <dc:subject>global change</dc:subject>
    <dc:subject>Ecosystem</dc:subject>
    <dc:subject>Soil acidification</dc:subject>
    <dc:subject>Civil and Structural Engineering</dc:subject>
    <dc:subject>Soil science</dc:subject>
    <dc:subject>2. Zero hunger</dc:subject>
    <dc:subject>Soil organic matter</dc:subject>
    <dc:subject>Soil Fertility</dc:subject>
    <dc:subject>Ecology</dc:subject>
    <dc:subject>Geography</dc:subject>
    <dc:subject>Soil Water Retention</dc:subject>
    <dc:subject>Life Sciences</dc:subject>
    <dc:subject>Cycling</dc:subject>
    <dc:subject>Forestry</dc:subject>
    <dc:subject>Carbon cycle</dc:subject>
    <dc:subject>04 agricultural and veterinary sciences</dc:subject>
    <dc:subject>15. Life on land</dc:subject>
    <dc:subject>Topsoil</dc:subject>
    <dc:subject>Soil carbon</dc:subject>
    <dc:subject>Chemistry</dc:subject>
    <dc:subject>Sink (geography)</dc:subject>
    <dc:subject>13. Climate action</dc:subject>
    <dc:subject>FOS: Biological sciences</dc:subject>
    <dc:subject>Environmental Science</dc:subject>
    <dc:subject>Physical Sciences</dc:subject>
    <dc:subject>Environmental chemistry</dc:subject>
    <dc:subject>0401 agriculture, forestry, and fisheries</dc:subject>
    <dc:subject>soil acidification</dc:subject>
    <dc:subject>Soil Carbon Dynamics and Nutrient Cycling in Ecosystems</dc:subject>
    <dc:subject>Research Article</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0001-6011-7591"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-3914-5402"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-4235-6438"/>
    <dc:creator>Xiaodong Song, Fei Yang, Huayong Wu, Jing Zhang, Decheng Li, Feng Liu, Yu-Guo Zhao, Jin-Ling Yang, Bing Ju, Chang Cai, Biao Huang, Huaiyu Long, Ying L&#252;, Yueyu Sui, Qiubing Wang, Kening Wu, Fengrong Zhang, Mingkui Zhang, Zhou Shi, Wenqi Ma, Gang Xin, Qi Zhang, Qingrui Chang, En Ci, Daoxian Yuan, Zhang Yang-zhu, Jun-Ping Bai, Jiaying Chen, Jie Chen, Yin-Jun Chen, Yun-Zhong Dong, Han Cui, Ling Li, Liming Li, Jianjun Pan, Fupeng Song, Fujun Sun, Dengfeng Wang, Tianwei Wang, Wei Xiang-hua, Hongqi Wu, Xia Zhao, Qing Zhou, Gan&#8208;Lin Zhang, </dc:creator>
    <dc:date>2021-07-02</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>Abstract                &lt;p&gt;Widespread soil acidification due to atmospheric acid deposition and agricultural fertilization may greatly accelerate soil carbonate dissolution and CO2 release. However, to date, few studies have addressed these processes. Here, we use meta-analysis and nationwide-survey datasets to investigate changes in soil inorganic carbon (SIC) stocks in China. We observe an overall decrease in SIC stocks in topsoil (0&#65506;&#65408;&#65427;30&#65474;&#65440;cm) (11.33&#65474;&#65440;g C m&#65506;&#65408;&#65427;2 yr&#65506;&#65408;&#65427;1) from the 1980s to the 2010s. Total SIC stocks have decreased by &#65506;&#65416;&#65468;8.99&#65474;&#65440;&#65474;&#65457;&#65474;&#65440;2.24% (1.37&#65474;&#65440;&#65474;&#65457;&#65474;&#65440;0.37&#65474;&#65440;Pg C). The average SIC losses across China (0.046 Pg C yr&#65506;&#65408;&#65427;1) and in cropland (0.016 Pg C yr&#65506;&#65408;&#65427;1) account for &#65506;&#65416;&#65468;17.6%&#65506;&#65408;&#65427;24.0% of the terrestrial C sink and 57.1% of the soil organic carbon sink in cropland, respectively. Nitrogen deposition and climate change have profound influences on SIC cycling. We estimate that &#65506;&#65416;&#65468;19.12%&#65506;&#65408;&#65427;19.47% of SIC stocks will be further lost by 2100. The consumption of SIC may offset a large portion of global efforts aimed at ecosystem carbon sequestration, which emphasizes the importance of achieving a better understanding of the indirect coupling mechanisms of nitrogen and carbon cycling and of effective countermeasures to minimize SIC loss.&lt;/p</dct:abstract>
    <dc:title>Significant loss of soil inorganic carbon at the continental scale</dc:title>
    <dc:identifier>PMC8824702</dc:identifier>
    <dct:references>https://doi.org/PMC8824702</dct:references>
    <dct:relation>818346</dct:relation>
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